{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362825894925973248.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/387275a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/387275a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/387275a0.pdf"}}],"dc:title":[{"@value":"Scour in large braided rivers and the recognition of sequence stratigraphic boundaries"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825894925973248","@type":"Researcher","foaf:name":[{"@value":"James L. Best"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894925973249","@type":"Researcher","foaf:name":[{"@value":"Philip J. Ashworth"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1997-05","prism:volume":"387","prism:number":"6630","prism:startingPage":"275","prism:endingPage":"277"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/387275a0"},{"@id":"http://www.nature.com/articles/387275a0.pdf"}],"createdAt":"2003-08-12","modifiedAt":"2023-05-18","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360846641639432960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A classification scheme for turbulence based on the velocity‐intermittency structure with an application to near‐wall flow and with implications for bed load transport"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367089648512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomorphological processes and their connectivity in hillslope, fuvial, and coastal areas in Bangladesh : a review"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792008805120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Formation of undulating topography and gravel beds at the bases of incised valleys : Last Glacial Maximum examples beneath the lowlands facing Tokyo Bay"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/387275a0"},{"@type":"CROSSREF","@value":"10.1029/2011jf002127_references_DOI_ReaoIOFR8hwyeSbclLTC0zQY1Zh"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00411-0_references_DOI_ReaoIOFR8hwyeSbclLTC0zQY1Zh"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00500-8_references_DOI_ReaoIOFR8hwyeSbclLTC0zQY1Zh"}]}